TY - JOUR AU - Haas, János AU - Hips, Kinga AU - Budai, Tamás AU - Győri, Orsolya AU - Lukoczki, Georgina AU - Kele, Sándor AU - Demény, Attila AU - Poros, Zsófia TI - Processes and controlling factors of polygenetic dolomite formation in the Transdanubian Range, Hungary: a synopsis JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 106 PY - 2017 IS - 3 SP - 991 EP - 1021 PG - 31 SN - 1437-3254 DO - 10.1007/s00531-016-1347-7 UR - https://m2.mtmt.hu/api/publication/3091740 ID - 3091740 N1 - MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/c, Budapest, 1117, Hungary Geological and Geophysical Institute of Hungary, Stefánia út 14, Budapest, 1143, Hungary Noble Research Center, Boone Pickens School of Geology, Oklahoma State University, Stillwater, OK 74078, United States Research Centre for Astronomy and Earth Sciences, Institute for Geological and Geochemical Research, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, 1112, Hungary ConocoPhillips Company, 600 N Dairy Ashford, Houston, TX 77079, United States Cited By :13 Export Date: 26 August 2022 CODEN: IJESF Correspondence Address: Haas, J.; MTA-ELTE Geological, Pázmány P. sétány 1/c, Hungary; email: haas@caesar.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Danišík, M AU - Fodor, László AU - Dunkl, István AU - Gerdes, A AU - Csizmeg, János AU - Hámorné, Vidó Mária AU - Evans, NJ TI - A multi-system geochronology in the Ad-3 borehole, Pannonian Basin (Hungary) with implications for dating volcanic rocks by low-temperature thermochronology and for interpretation of (U-Th)/He data JF - TERRA NOVA J2 - TERRA NOVA VL - 27 PY - 2015 IS - 4 SP - 258 EP - 269 PG - 12 SN - 0954-4879 DO - 10.1111/ter.12155 UR - https://m2.mtmt.hu/api/publication/2922731 ID - 2922731 N1 - Funding Agency and Grant Number: Hungarian Scientific Research Found [42799]; Austrian-Hungarian Action Foundation [68ou7] Funding text: The study was supported by the Hungarian Scientific Research Found No. 42799 and Austrian-Hungarian Action Foundation No 68ou7. Part of the stratigraphical column was drawn by Z. Lantos (Budapest), and O. Sztano (Budapest) contributed to sedimentological interpretation. Finally, we thank an anonymous reviewer, C. Persano, F. Horvath, and the associate editor Meinert Rahn for detailed and constructive reviews. LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Budai, Tamás AU - Raucsik, Béla TI - Climatic controls on sedimentary environments in the Triassic of the Transdanubian Range (Western Hungary) JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 353-355 PY - 2012 SP - 31 EP - 44 PG - 14 SN - 0031-0182 DO - 10.1016/j.palaeo.2012.06.031 UR - https://m2.mtmt.hu/api/publication/2048753 ID - 2048753 N1 - Cited By :48 Export Date: 26 August 2022 CODEN: PPPYA Correspondence Address: Raucsik, B.; Department of Geology, Ifjúság útja 6, H-7624 Pécs, Hungary; email: raucsik.bela@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Hips, Kinga AU - Haas, János TI - Facies and diagenetic evaluation of the Permian-Triassic boundary interval and basal Triassic carbonates: shallow and deep ramp sections, Hungary. JF - FACIES J2 - FACIES VL - 55 PY - 2009 IS - 3 SP - 421 EP - 442 PG - 22 SN - 0172-9179 DO - 10.1007/s10347-009-0182-8 UR - https://m2.mtmt.hu/api/publication/152141 ID - 152141 N1 - Cited By :17 Export Date: 27 January 2023 Correspondence Address: Hips, K.; Geological, Geophysical and Space Science Research Group, Pázmány s. 1/c, 1117 Budapest, Hungary; email: hips@ludens.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Csontos, L AU - Vörös, Attila TI - Mesozoic plate tectonic reconstruction of the carpathian region JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 210 PY - 2004 IS - 1 SP - 1 EP - 56 PG - 56 SN - 0031-0182 DO - 10.1016/j.palaeo.2004.02.033 UR - https://m2.mtmt.hu/api/publication/1236932 ID - 1236932 N1 - Cited By :483 Export Date: 11 November 2022 CODEN: PPPYA Correspondence Address: Csontos, L.; Geological Department, Pazmany P: setany 1/a, Budapest 1117, Hungary; email: csontos@ludens.elte.hu Funding details: Hungarian Science Foundation, T 037595, T 043760 Funding text 1: The authors are indebted to many colleagues for the discussions of earlier oral and written versions of the manuscript. We would like to thank especially F. Horváth, A. Galácz, S. Kovács, M. Kázmér, E. Márton (Budapest), D. Plašienka, M. Kováč (Bratislava), F. Neubauer and Č. Tomek (Salzburg), K. Birkenmajer (Kraków), M. Săndulescu (Bucharest) S. Schmid (Basel) and P. Ziegler (Basel). We express our thanks to W. Frisch, F. Horváth, G. Stampfli, Alonso-Gutierrez, J. Von Raumer, B. Murphy, A. Collins and D. Nance who kindly revised and improved earlier versions of the manuscript. This version was helped by critical remarks of K. Birkenmajer, F. Neubauer, B. Sperner, G. Stampfli, and F. Surlyk. IGCP project 453 is gratefully thanked for moral and material support. Hungarian Science Foundation OTKA projects T 043760, T 037595 are also thanked for support. AB - Palaeomagnetic, palaeobiogeographic and structural comparisons of different parts of the Alpine-Carpathian region suggest that four terranes comprise this area: the Alcapa, Tisza, Dacia and Adria terranes. These terranes are composed of different Mesozoic continental and oceanic fragments that were each assembled during a complex Late Jurassic-Cretaceous Palaeogene history. Palaeomagnetic and tectonic data suggest that the Carpathians are built up by two major oroclinal bends. The Alcapa bend has the Meliata oceanic unit, correlated with the Dinaric Vardar ophiolite, in its core. It is composed of the Western Carpathians, Eastern Alps and Southern Alcapa units (Transdanubian Range, Bukk). This terrane finds its continuation in the High Karst margin of the Dinarides. Further elements of the Alcapa terrane are thought to be derived from collided microcontinents: Czorsztyn in the N and a carbonate unit (Tisza?) in the SE. The Tisza-Dacia bend has the Vardar oceanic unit in its core. It is composed of the Bihor and Getic microcontinents. This terrane finds its continuation in the Serbo-Macedonian Massif of the Balkans. The Bihor-Getic microcontinent originally laid east of the Western Carpathians and filled the present Carpathian embayment in the Late Palaeozoic-Early Mesozoic. The Vardar ocean occupied an intermediate position between the Western Carpathian-Austroalpine-Transdanubian-High Karst margin and the Bihor-Getic-Serbo-Macedonian microcontinent. The Vardar and Pindos oceans were opened in the heart of the Mediterranean-Adriatic microcontinent in the Late Permian-Middle Triassic. Vardar subducted by the end of Jurassic, causing the Bihor-Getic-Serbo-Macedonian microcontinent to collide with the internal Dinaric-Western Carpathian margin. An external Penninic-Vahic ocean tract began opening in the Early Jurassic, separating the Austroalpine-Western Carpathian microcontinent (and its fauna) from the European shelf. Further east, the Severin-Ceahlau-Magura also began opening in the Early Jurassic, but final separation of the Bihor-Getic ribbon (and its fauna) from the European shelf did not take place until the late Middle Jurassic. The Alcapa and the Tisza-Dacia were bending during the Albian-Maastrichtian. The two oroclinal bends were finally opposed and pushed into the gates of the Carpathian embayment during the Palaeogene and Neogene. At that time, the main NS shortening in distant Alpine and Hellenic sectors was linked by a broader right-lateral shear zone along the former Vardar suture. (C) 2004 Elsevier B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Budai, Tamás TI - Triassic sequence stratigraphy of the Transdanubian Range (Hungary) JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 50 PY - 1999 IS - 6 SP - 459 EP - 475 PG - 17 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/1019032 ID - 1019032 N1 - Cited By :50 Export Date: 19 January 2023 Correspondence Address: Haas, J.; Academic Research Group, Muzeum korut 4/a, H-1088 Budapest, Hungary AB - On the basis of surface exposures and core sections, a comprehensive sequence analysis of the Triassic series was carried out in the Transdanubian Range. For recognition of the sequences as well as their boundaries, the regional subaerial exposure horizons, the maximum flooding intervals, the transgressive-regressive trends, the platform progradations and backsteppings, as well as signals of the higher order accommodation changes were primarily considered. Detailed analyses were accomplished in six selected sub-regions. On the basis of the results of these analyses, a composite sequence chart was compiled. The Triassic history of the Transdanubian Range can be subdivided into four stages. Within the first stage (Induan to Middle Anisian) which can be characterized by a ramp setting, five sequences have been recognized. The second stage (Middle Anisian-Ladinian) is mainly controlled by the Neotethys rifting and can be subdivided into three sequences. Infilling of the previously formed basins took place during the third stage (Carnian), consisting of three sequences. The fourth stage (latest Carnian to Rhaetian) reflects the passive margin evolution of the Neotethys. However, a new rifting (Ligurian-Penninic) began in the Late Norian and also influenced the evolution of the Transdanubian Range. Four sequences were recognized in this final evolutionary stage. About 50 % of the recognized sequence boundaries could be correlated with those reported from the Southern and Northern Alps, from the German Basin, and from Western Canada. LA - English DB - MTMT ER - TY - JOUR AU - Budai, Tamás AU - Haas, János TI - Triassic sequence stratigraphy of the Balaton Highland, Hungary JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 40 PY - 1997 IS - 3 SP - 307 EP - 335 PG - 29 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1025551 ID - 1025551 N1 - Cited By :23 Export Date: 3 December 2018 LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Kovács, Sándor AU - Krystyn, L AU - Lein, R TI - Significance of Late Permian-Triassic facies zones in terrane reconstructions in the Alpine-North Pannonian domain JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 242 PY - 1995 IS - 1-2 SP - 19 EP - 40 PG - 22 SN - 0040-1951 DO - 10.1016/0040-1951(94)00157-5 UR - https://m2.mtmt.hu/api/publication/1019016 ID - 1019016 N1 - Geological Research Group, the Hungarian Academy of Sciences, Múzeum krt. 4 / a, 1088 Budapest, Hungary University of Vienna, Department of Palaeontology, Universitätstr. 7, A-1010 Wien, Austria University of Vienna, Department of Geology, Universitätstr. 7, A-1010 Wien, Austria Cited By :245 Export Date: 28 August 2023 Correspondence Address: Haas, J.; Geological Research Group, the Hungarian Academy of Sciences, Múzeum krt. 4 / a, 1088 Budapest, Hungary AB - The present-day setting of the tectonic units (terranes) making up the pre-Neogene basement of the Pannonian Basin and the West Carpathians is the result of large-scale displacements during the Alpine collisional phases. To explain this setting, based on various concepts, a number of models have been proposed in the last decade. Most of them agree in an eastward escape of the ''North Pannonian terrane'' from the Alpine domain towards the Pannonian during the Palaeogene-Early Miocene period. In the present paper a reconstruction of the pre-escape setting of the displaced terranes is presented based on facies zones in selected time-slices from the Late Permian to the Late Triassic. According to our reconstruction the Inner West Carpathian units were located east of the Austroalpine units forming the northern shelf of the ''Euhallstatt''-Meliatic basin of the Vardar oceanic branch. The Drauzug should have been located in a position much more external than its present-day setting. The Transdanubian Range was situated in the northern neighbourhood of the Southern Alps, whereas the Bukk may have been located adjacent to the NW Dinarides. The Mid-Transdanubian zone is a major shear-zone containing elements of the Julian Alps and Sava folds nappe system and the Inner Dinaric ophiolitic melange. Although the nappe-tectonism may have played an important role in the structural evolution of the ''North Pannonian terrane'', this mechanism alone can hardly produce hundreds of kilometres of facies offset on the opposite sides of strike-slip zones. LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Budai, Tamás TI - Upper Permian-Triassic facies zones in the Transdanubian Range JF - RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA J2 - RIV IT PALEON STRATIG VL - 101 PY - 1995 IS - 3 SP - 249 EP - 266 PG - 18 SN - 0035-6883 UR - https://m2.mtmt.hu/api/publication/1019017 ID - 1019017 LA - English DB - MTMT ER - TY - JOUR AU - CSONTOS, L AU - Nagymarosy, András AU - Horváth, Ferenc AU - KOVAC, M TI - TERTIARY EVOLUTION OF THE INTRA-CARPATHIAN AREA - A MODEL JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 208 PY - 1992 IS - 1-3 SP - 221 EP - 241 PG - 21 SN - 0040-1951 DO - 10.1016/0040-1951(92)90346-8 UR - https://m2.mtmt.hu/api/publication/1255443 ID - 1255443 N1 - Eötvös University of Budapest, Department of Geology, 1088 Budapest, Múzeum krt. 4 / a, Hungary Eötvös University of Budapest, Department of Geophysics, 1082 Budapest, Ludovika tér 2, Hungary Slovakian Academy of Sciences, Department of Geology, 81473 Bratislava, Dúbravska cesta, Czechoslovakia Cited By :473 Export Date: 11 November 2022 Correspondence Address: Csontos, L. AB - The Outer Carpathian flysch nappes encircle an Intra-Carpathian domain which can be divided into two megatectonic units (North Pannonian and Tisza) mostly on the basis of contrasting Mesozoic and Palaeogene facies development. We see two major kinematic problems to be solved: (1) The present distribution of the Mesozoic and Palaeogene facies is mosaic-like, and some belts form exotic bodies within realms of Austroalpine affinity. (2) Late Eocene palinspastic reconstruction of the Outer Carpathian flysch nappes suggest, that the entire Intra-Carpathian area must have been located several hundreds of kilometres to the south and to the west of its present position. Neogene extension can account for shortening in the external Carpathian nappes, but is unable to explain Mesozoic facies anomalies and offsets of Palaeogene formations. We suggest that evolution of the Intra-Carpathian area involved first Late Palaeogene-Early Miocene juxtaposition of the North-Pannonian and Tisza megatectonic units, accompanied by the closure of the external Carpathian flysch troughs; thereafter extension of this amalgamated unit occurred, which was compensated by thrusting of flysch nappes onto the European foreland and formation of molasse foredeeps. Eastward escape of the North-Pannonian unit from the Alpine collisional belt involved left lateral shear along the Pieniny Klippen belt and right lateral shear along the Mid-Hungarian zone. Parts of the Late Palaeogene basin and an Early Miocene volcanic edifice were dissected, offset and elongated by several 100 kms. The driving mechanism of the eastward escape of the Intra-Carpathian area can be related to the collision of Apulia and Europe and the subduction of the external Carpathian crust under the Pannonian units. The escape ceased gradually in the Early Miocene, when oblique collision between the North-Pannonian unit and European continent occurred. Neogene extension of the Pannonian region was an areal deformation. The extension at locally variable rate resulted in the break-up of the heterogenous floor of the Neogene basin. The driving mechanism of basin extension and contemporaneous compressional deformation of the external Carpathians is thought to be related to ongoing subduction, involving the marginal part of the attenuated European continental crust. Tectonic activity in the Carpathians and basin subsidence and volcanism shifted in time and in unison from the west toward the east-southeast. LA - English DB - MTMT ER -